生态环境学报 ›› 2026, Vol. 35 ›› Issue (4): 520-528.DOI: 10.16258/j.cnki.1674-5906.2026.04.003
崔志攀(
), 张绍兵, 张西哲, 韩艳英, 吴正, 仝令臣, 叶彦辉*(
)
收稿日期:2025-10-08
修回日期:2026-02-03
接受日期:2026-03-02
出版日期:2026-04-18
发布日期:2026-04-14
通讯作者:
*E-mail: 作者简介:崔志攀(1997年生),男,硕士研究生,主要从事高寒草地氮磷沉降研究。E-mail: 1723957643@qq.com
基金资助:
CUI Zhipan(
), ZHANG Shaobing, ZHANG Xizhe, HAN Yanying, WU Zheng, TONG Lingchen, YE Yanhui*(
)
Received:2025-10-08
Revised:2026-02-03
Accepted:2026-03-02
Online:2026-04-18
Published:2026-04-14
摘要:
由于人类活动和工业发展活性氮磷的输入持续增多。目前,色季拉山高寒草地还缺乏氮磷富集下土壤理化性质的研究,且较少关注氮磷的交互作用。以色季拉山高寒草地为对象,通过开展野外氮磷添加控制实验,探究土壤酶活性和化学计量比对养分添加的响应机制。结果显示,1)相较对照,氮磷复合添加下β-1,4-葡萄糖苷酶与纤维二糖水解酶分别上升71.3%与62.0%(p<0.05);氮获取酶呈“异向”响应:β-1,4-N-乙酰基氨基葡萄糖苷酶在磷与氮磷下显著升高90.6%、59.8%,在氮处理下降43.8%;亮氨酸氨基肽酶仅在氮磷复合处理下显著升高111%;碱性磷酸酶主要在氮磷复合处理下上升55.2%(p<0.05)。2)酶化学计量与矢量分析表明,微生物总体受磷限制:各处理矢量角均大于45°;氮磷虽提升群落代谢上限,但主导限制仍偏向磷端。3)相关分析与冗余分析显示,外源氮、磷及氮磷通过改变土壤碳氮比、有效磷、微生物量碳与有机碳供给等因子共同调控酶与酶计量结构;磷与氮磷下有效磷显著提高103%、427%,微生物量碳在氮磷处理下降低了32.9%,溶解性有机碳氮磷处理下降低8.21%,样点沿“有效磷-碳氮比”梯度清晰分离(p<0.05)。综上所述,该研究揭示了高寒草地在氮、磷富集下的“计量再平衡-代谢阈值”特征:单因子添加改变特定位点的“酶学投资”,复合添加放大代谢潜力但仍未改变磷主导限制。
中图分类号:
崔志攀, 张绍兵, 张西哲, 韩艳英, 吴正, 仝令臣, 叶彦辉. 氮磷添加对色季拉山高寒草地土壤酶活性和化学计量比的影响[J]. 生态环境学报, 2026, 35(4): 520-528.
CUI Zhipan, ZHANG Shaobing, ZHANG Xizhe, HAN Yanying, WU Zheng, TONG Lingchen, YE Yanhui. Effects of Nitrogen and Phosphorus Addition on Soil Enzyme Activity and Stoichiometric Ratios in the Alpine Grassland of Sejila Mountain[J]. Ecology and Environmental Sciences, 2026, 35(4): 520-528.
| 参数 | 对照 | 氮添加 | 磷添加 | 氮磷复合添加 |
|---|---|---|---|---|
| pH | 5.83±0.01a | 5.39±0.01d | 5.43±0.01c | 5.66±0.01b |
| 容重/(g‧cm−3) | 0.76±0.01b | 0.74±0.02b | 0.75±0.03b | 1.09±0.05a |
| w(有机碳)/(g‧kg−1) | 49.78±2.82b | 67.09±4.38a | 71.00±3.67a | 46.16±0.97b |
| w(总氮)/(g‧kg−1) | 4.11±0.27b | 5.53±0.48a | 5.64±0.33a | 4.20±0.09b |
| w(总磷)/(mg‧kg−1) | 0.81±0.03c | 0.91±0.01b | 1.07±0.01a | 0.90±0.02b |
| 碳氮比 | 12.14±0.13a | 12.20±0.40a | 12.59±0.09a | 11.00±0.16b |
| 碳磷比 | 61.92±4.26ab | 73.63±4.65a | 66.28±2.95a | 51.67±2.03b |
| 氮磷比 | 5.11±0.37ab | 6.07±0.55a | 5.27±0.27ab | 4.70±0.15b |
表1 氮磷添加对高寒草地土壤理化性质的影响
Table 1 Effects on N and P additions on the physice-chemical properties of alpine grassland soils
| 参数 | 对照 | 氮添加 | 磷添加 | 氮磷复合添加 |
|---|---|---|---|---|
| pH | 5.83±0.01a | 5.39±0.01d | 5.43±0.01c | 5.66±0.01b |
| 容重/(g‧cm−3) | 0.76±0.01b | 0.74±0.02b | 0.75±0.03b | 1.09±0.05a |
| w(有机碳)/(g‧kg−1) | 49.78±2.82b | 67.09±4.38a | 71.00±3.67a | 46.16±0.97b |
| w(总氮)/(g‧kg−1) | 4.11±0.27b | 5.53±0.48a | 5.64±0.33a | 4.20±0.09b |
| w(总磷)/(mg‧kg−1) | 0.81±0.03c | 0.91±0.01b | 1.07±0.01a | 0.90±0.02b |
| 碳氮比 | 12.14±0.13a | 12.20±0.40a | 12.59±0.09a | 11.00±0.16b |
| 碳磷比 | 61.92±4.26ab | 73.63±4.65a | 66.28±2.95a | 51.67±2.03b |
| 氮磷比 | 5.11±0.37ab | 6.07±0.55a | 5.27±0.27ab | 4.70±0.15b |
图2 氮、磷添加对高寒草地土壤养分和微生物量的影响 CK:对照组:氮添加;P:磷添加;NP:氮磷复合添加;不同小写字母表示处理间差异显著(p<0.05),样本重复数n=3。下同
Figure 2 Effects of N and P addition on soil nutrients and microbial biomass in alpine grassland
图5 土壤酶活性和酶计量比与理化因子之间的关系 BD:容重;SOM:土壤有机碳;TP:总磷;TN:总氮;C?N?碳氮比;C?P?碳磷比;N?P?氮磷比;AP:有效磷;AN:有效氮;DOC:可溶性有机碳;CMB:微生物碳;NMB:微生物氮;PMB:微生物磷;VA:矢量角度;VL:矢量长度;CAE:碳获取酶;NAE:氮获取酶;PAE:磷获取酶;Ecn:酶碳氮比;Ecp:酶碳磷比;Enp:酶氮磷比;BG:β-1,4葡萄糖苷酶;CBH:纤维二糖水解酶;NAG:B-1,4N-乙酰氨基葡萄糖苷酶;LAP:亮氨酸氨基肽酶;ALP:碱性磷酸酶;CK:对照组;N:氮添加;P:磷添加;NP:氮磷复合添加,样本重复数n=3
Figure 5 Soil enzyme activities and enzyme stoichiometric ratios in relation to physico-chemical factors
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